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首页> 外文期刊>Journal of Physics. Condensed Matter >Comparison between theory and simulations for the magnetization and the susceptibility of polydisperse ferrofluids
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Comparison between theory and simulations for the magnetization and the susceptibility of polydisperse ferrofluids

机译:多分散铁磁流体的磁化和磁化率理论与模拟的比较

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摘要

The influence of polydispersity on the magnetization of ferrofluids is studied based on a previously published magnetization equation of state (Szalai and Dietrich, 2011 J. Phys.: Condens. Matter 23 326004) and computer simulations. The polydispersity of the particle diameter is described by the gamma distribution function. Canonical ensemble Monte Carlo simulations have been performed in order to test these theoretical results for the initial susceptibility and the magnetization. The results for the magnetic properties of the polydisperse systems turn out to be in quantitative agreement with our present simulation data. In addition, we find good agreement between our theory and experimental data for magnetite-based ferrofluids.
机译:基于先前公布的磁化状态方程(Szalai和Dietrich,2011 J. Phys.:Condens。Matter 23 326004)和计算机模拟研究了多分散性对铁磁流体磁化的影响。粒径的多分散性由伽马分布函数描述。为了测试这些理论结果的初始磁化率和磁化强度,已进行了典型的合奏蒙特卡洛模拟。结果表明,多分散体系的磁性能结果与我们目前的模拟数据在定量上吻合。此外,我们发现基于磁铁矿的铁磁流体的理论和实验数据之间有很好的一致性。

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